A new world-class deep-water play-type, deposited by the syndepositional interaction of turbidity flows and bottom currents: The giant Eocene Coral Field in northern Mozambique. (January 2020)

• Record Type: Journal Article
• Authors: Fonnesu, Marco; Palermo, Denis; Galbiati, Mauro; Marchesini, Marco; Bonamini, Enrico; Bendias, Daniel
• Is Part Of: Marine and petroleum geology. Volume 111(2020)
• Page Start: 179
• Page End: 201
• Publication Date: 2020-01
• Subjects: Deep-water -- Turbidites -- Contourites -- Channels -- Play -- Rovuma basin -- Coral field -- Reservoir modelling; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2019.07.047
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: The discovery of the super-giant Coral and Mamba gas fields in the offshore of Northern Mozambique provides a unique insight into the architecture of a new deep-water play-type. High-quality seismic and extensive well data from both fields shows that very clean (clay matrix-poor) sandstone reservoirs, with thickness >100 m and extended over tens of km can be formed by the syndepositional interaction of down-slope high-density turbulent gravity flows and across-slope bottom currents. This is recorded by: i) the marked asymmetry of submarine channels and lateral stacking in which top-of-fan seismic reflectors show a lateral transition from high to low amplitude response from axis to off-axis locations; ii) the occurrence of laterally-deviated lobe deposits, sediment waves and channel-associated drifts in the inferred bottom current direction; iii) the presence of very clean sandstones forming the bulk of the fan units and the consistent lack of interbedded fine-grained facies; iv) the occurrence of fine-grained and thin-bedded facies adjacent to the main fan axes, which are characterized by repeated transitions between ripples and parallel-laminated sandstones, mud-drapes, shale clasts and bi-directional cross-laminae in the same bed, indicating intense traction and velocity pulsations. This association forms a mixed depositional system, in which only the basal and coarse-grained part of the turbidity current load is deposited and preserved in the axial part of the system, whilst all the finer-grained sediments are pirated from the turbulent cloud by laterally flowing bottom currents and deposited in the adjacent sediment drifts. The inferred process results in exceptionally high quality reservoirs whose architectural and facies models were confirmed by the appraisal campaign and production well tests and incorporated into the reservoir model. The results of this study indicate a significant exploration potential in similar geological settings and the definition of a potential new play type, that could lead to the reinterpretation of existing deep-water datasets. Highlights: First insight of the Area 4 in northern Mozambique and the Coral Field. New deep-water play-type: very thick, clean and extensive reservoir sandstones. Deposits formed by syndepositional interaction of bottom currents and gravity flows. High quality dataset composed of well logs, cores and 3D seismic. A facies tract related to deposits affected by bottom currents is proposed.